Transcription

Down Farnborough Kent

June 7th—

My dear Lyell

I was in London for the last Geological, & found at
my Brother's two pamphlets from you, one most useful to me, &
a packet of Maple Sugar for Lizzie, which pleased her much; & by a great effort
she agreed to send you her many thanks;—poor little dear, graciosity, as yet,
is not her forte. I make the above facts an excuse for writing
to you, for I have very little to say. I was extremely sorry to hear of the delay in the
opening of the Exhibition; but I hope it will not interfere
with the Canary Islands.—

I went up for a Paper by the Arctic Dr
Sutherland on ice-action, read only in abstract, but I
shd think with much good matter. It was very pleasant to hear, that it was written owing to the
admiralty manual. There was also a paper by Trimmer partly on
the superficial deposits of Kent, Murchison urged his
catastrophe view to account for the flints, so I gave your
view of sub-glacial action & urged where on earth the flood, which divided
France & England, could have found so vast a pile of almost clean flints. I
stated that one of the arctic navigators, had informed you that the stones on the beach
were angular in those countries: & on this head I asked
Dr. Sutherland, & he most strongly
confirmed this statement; & I thought you would like to hear this. Hopkins spoke, he admitted to a
considerable extent, the force of my notion of (plastic) icebergs being driven by their
momentum over considerable inequalities in an almost straight course. Chambers also spoke at length: Have you seen his long & I must say
interesting Paper on glaciation in Eding. New. Phil Journal: he actually reproduces
Agassiz's notion of one continuous sheet of ice over the whole northern world,
& treats all Icebergians with the most supercilious contempt.—

I do not know whether you will care to hear the above Report of our meeting; but I do
not at all expect you to answer this.—

I did not stay for the battle royal at the Royal
Socy but I see Murchison & Beaufort
gained the day, & Capt Inglefield was elected making one more than the proper
number of admissions.

We are all well: I am alone at present; Emma having gone for a few days to her
sisters. On July
1st we go for a month, the whole posse
comitatus of us, to the Isle of Wight: & on our
return I hope to go to press with my weariful cirripedes.

Elizabeth Darwin, nearly 6 years old, was slow in developing as a child and
was not able to live a fully independent adult life. Very little is known about her, but
in the notebook in which observations on the Darwin children are recorded, Emma noted
that Elizabeth's speech at 412 years old was confused; her pronunciation was strange and her phraseology
peculiar. By the time she was 5 years old, she had developed ‘a great
habit of abstraction going by herself & talking to herself for an hour. She does
not like to be interrupted’. (Correspondence vol. 4,
Appendix III, MS pp. 42–42v.) In his letter to W. E. Darwin,
24 [February 1852], CD reported that Elizabeth ‘shivers & makes as
many extraordinary grimaces as ever’. Elizabeth lived with CD and Emma in Down
and, after CD's death, remained with Emma in Cambridge and Down (Wedgwood and
Wedgwood 1980, pp. 321–2; Emma Darwin (1904),
p. 338). Following Emma's death, she settled in Cambridge. Her sister
Henrietta Litchfield, included letters concerning Elizabeth's voluntary work in
1891 at the infirmary of the workhouse in Cambridge in Emma Darwin
(1904), 2: 404–5. In the later edition of Emma Darwin (1915), she
noted only Elizabeth's birth. Gwen Raverat, CD's granddaughter, who
knew Elizabeth towards the end of her life in the 1920s, observed: ‘She was
not good at practical things … and she could not have managed her own life
without a little help and direction now and then; but she was shrewd enough in her own
way, and a very good judge of character.’ (Raverat 1952,
pp. 146–7). See also Darwin 1955, pp. 58–9.

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f3 1518.f3

Lyell, a permanent member of the Royal Commission for the Exhibition of 1851, had
been asked by the Government to represent science at the New York Industrial Exhibition
of 1853 (K. M. Lyell ed. 1881, 2: 187–8). This letter is addressed to
Lyell as ‘Commissioner to the Great Exhibition | New York
| U.S.’

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f4 1518.f4

Lyell intended to visit the islands in the autumn of 1853 (K. M. Lyell ed.
1881, 2: 188). However, the trip was not made until February 1854 (see letter to
J. D. Dana, 6 December [1853], n. 13).

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f5 1518.f5

Peter Cormack Sutherland served as surgeon on several Arctic expeditions. His paper,
Sutherland 1853, was communicated to the Geological Society by Andrew Crombie
Ramsay.

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f6 1518.f6

A manual of scientific enquiry (Herschel ed. 1849), intended to direct
naval officers in their scientific investigations, to which CD had contributed the
chapter on geology.

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f7 1518.f7

Trimmer 1853, the third part of Joshua Trimmer's work on the origin of the
soils which cover the Chalk of Kent.

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f8 1518.f8

The flints are described in Trimmer 1853, pp. 289–90. For
Roderick Impey Murchison's views on the catastrophic origin of the flint drift,
see Murchison 1851 which refers to Trimmer 1851, the first part of
Trimmer's work on the origin of the soils which cover the Chalk of Kent.

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f9 1518.f9

According to Lyell (and CD), flints and erratic boulders were dropped by icebergs or
by local glaciers: flints transported by floods or by surf action on beaches would be
rounded. For Murchison's argument against the agency of ice in the formation of
the drift deposits, see Murchison 1851, p. 395. The angular nature of the
flints, according to Murchison, indicated ‘a much greater intensity of
fracture in former stages of the planet than now’ and that ‘such
dislocations must have been accompanied by torrents of water’;
‘ordinary tidal action’, he argued, would have produced
‘water-worn pebbles’ (Murchison 1851, p. 394).

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William Hopkins.

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f11 1518.f11

CD eventually published a paper in 1855 on the plasticity of icebergs and
their power to make rectilinear grooves across a submarine undulatory surface
(Collected papers 1: 252–5).

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f12 1518.f12

Chambers 1853a, in which Robert Chambers stated: ‘If any man were to say,
that because he can with some difficulty smooth a rough surface of wood with his
thumb-nail, therefore his dining-tables must have been fashioned and polished by the
joiner with that little instrument alone, I would consider him as advancing a theory
fully as tenable as that which consists in attributing all the so-called glacial
phenomena to ice-bergs.’ (p. 230).

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f13 1518.f13

The Royal Society council meeting for the nomination of fellows took place on
2 June 1853 (Abstracts of the papers communicated to theRoyal Society of London 6 (1850–4): 311–12). On this day,
sixteen scientific men, including Captain Edward Augustus Inglefield, were elected FRS
instead of the fifteen stipulated as the maximum in the rules of the society (Hall 1984,
pp. 80–2). Murchison and Francis Beaufort presumably had proposed
Inglefield.

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Elizabeth Wedgwood and Charlotte Langton. Both lived in Hartfield, Sussex. Emma
noted in her diary that she went to Hartfield on 6 June and returned home on
10 June.

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f15 1518.f15

This plan was changed. Instead, on 14 July, the family took a house in
Eastbourne, Sussex (‘Journal’; Correspondence
vol. 5, Appendix I).